Zobrazeno 1 - 10
of 45
pro vyhledávání: '"ERIK WOLFGRING"'
Autor:
Erik Wolfgring, Michael Wagreich
Publikováno v:
PeerJ, Vol 4, p e1757 (2016)
Deposits spanning the Radotruncana calcarata Taxon Range Zone at the Postalm section, Northern Calcareous Alps (Austria) are examined quantitatively for foraminiferal assemblages, especially the planktonic group. This study focuses on establishing a
Externí odkaz:
https://doaj.org/article/72d99dd6cf514b65a5e091b198176c9d
Autor:
Antonino Briguglio, Victor Manuel Giraldo-Gómez, Andrea Baucon, Andrea Benedetti, Cesare Andrea Papazzoni, Johannes Pignatti, Erik Wolfgring, Michele Piazza
Publikováno v:
Newsletters on Stratigraphy.
Autor:
Maria Rose Petrizzo, Giulia Amaglio, Erik Wolfgring, David K. Watkins, Kenneth G. MacLeod, Brian T. Huber, Takashi Hasegawa
Oceanic Anoxic Event 2 (OAE 2), spanning the Cenomanian/Turonian boundary (93.9 Ma) was an episode of major perturbations in the global carbon cycle with a δ13C excursion of 2-3‰ documented worldwide. To investigate the response of biota to OAE 2
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5a3ead69e81fd097d0babb9bd99f7e8b
https://doi.org/10.5194/egusphere-egu23-7874
https://doi.org/10.5194/egusphere-egu23-7874
At Site U1516 (Mentelle Basin, southeast Indian Ocean, offshore western Australia), the International Ocean Discovery Program (IODP) Expedition 369 recovered an almost complete record of the Upper Cretaceous, including the Oceanic Anoxic Event 2 (OAE
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5d02e5b455df9abe5a794d83e8e0d769
https://doi.org/10.5194/egusphere-egu23-11574
https://doi.org/10.5194/egusphere-egu23-11574
The Cenomanian-Turonian boundary interval is characterized by environmental perturbations related to the Oceanic Anoxic Event 2 (OAE 2), affecting marine biota, including benthic and planktonic foraminifera. This study shows a continuous record of be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b3453d1cfdbea5829c821face7f61863
https://doi.org/10.5194/egusphere-egu23-6659
https://doi.org/10.5194/egusphere-egu23-6659
Autor:
MARCOS ANTONIO BATISTA DOS SANTOS FILHO, GERSON FAUTH, BENJAMIN SAMES, ERIK WOLFGRING, JORGE VILLEGAS-MARTÍN
Publikováno v:
PALAIOS. 36:356-376
This paper presents the results of a paleoenvironmental study of two Hauterivian–Aptian adjacent sections (Transnordestina A/B) of the Iguatu Basin using ostracods and aided by X-ray fluorescence (XRF), total organic carbon (TOC), total sulfur (S),
Autor:
Maria Rose Petrizzo, Giulia Amaglio, David K. Watkins, Kenneth G. MacLeod, Brian T. Huber, Takashi Hasegawa, Erik Wolfgring
Publikováno v:
Paleoceanography and Paleoclimatology. 37
Oceanic Anoxic Event 2, spanning the Cenomanian/Turonian boundary (93.9 Ma), was an episode of major perturbations in the global carbon cycle. To investigate the response of biota and the paleoceanographic conditions across this event, we present dat
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 623:111598
Autor:
T. M. Quan, Trine Edvardsen, Matthew M. Jones, Yongxiang Li, R. do Monte Guerra, Sietske J. Batenburg, Z. Xu, Tao Jiang, Hans-Juergen Brumsack, Mathieu Martinez, Kara Bogus, Maria Luisa G. Tejada, Dennis L. Harry, Kirsty M. Edgar, Gabriel Tagliaro, Maria Rose Petrizzo, Eun Lee, Laurent Riquier, Carmine C. Wainman, Shannon J. Haynes, Lloyd T. White, A Maritati, Carl Richter, Erik Wolfgring, L.K. O’Connor, Richard Hobbs, Brian T. Huber, David K. Watkins, Kenneth G. MacLeod, Junichiro Kuroda, Takashi Hasegawa
Publikováno v:
Gondwana Research
Gondwana Research, 2020, 83, pp.80-95. ⟨10.1016/j.gr.2020.01.009⟩
Gondwana Research, Elsevier, 2020, 83, pp.80-95. ⟨10.1016/j.gr.2020.01.009⟩
Gondwana Research, 2020, 83, pp.80-95. ⟨10.1016/j.gr.2020.01.009⟩
Gondwana Research, Elsevier, 2020, 83, pp.80-95. ⟨10.1016/j.gr.2020.01.009⟩
International audience; The Upper Cretaceous sedimentary sequence at International Ocean Discovery Program Site U1512 in the Ceduna Sub-basin of the Great Australian Bight represents a continuous, > 690 m thick interval of black silty clay and clayst